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微尺度电流对变化的海洋生物地质化学循环的影响

Marina Lévy¹, Damien Couespel², Clément Haëck¹

¹Sorbonne Université, Laboratoire d'Océanographie et du Climat: Expérimentations et Analyses Numériques de l'Institut Pierre Simon Laplace (LOCEAN-IPSL), CNRS/IRD/MNHN, Paris, France;

Annual review of marine science

|June 23, 2023

概括

微小的海洋流对生物地化学循环产生重大影响,影响营养物质的运输和气候变化影响. 了解这些小规模的过程对于准确的气候预测和海洋学研究至关重要.

科学领域:

海洋学海洋学海洋学
生物地质化学生物地质化学
气候科学气候科学

背景情况:

微小的海洋流 (1-100公里,数天-数月) 是生物地化学标记物运输和转化的关键驱动因素.
由于多层次复杂性,这些电流对每年生物地球化学循环的大规模影响仍然不太了解.

研究的目的:

总结和批判性地审查微量流对大规模海洋生物地化学循环的影响.
检查流和高档连接在生物地球化学标记物平衡中的作用.
突出微小尺度在低频变化和气候变化缓冲中的重要性.

主要方法:

对细度海洋动力学和生物地球化学过程的现有文献的审查.
分析流和高层连接如何影响大规模的生物地化学预算.
评估细在自然变化和气候变化影响中的作用.

主要成果:

与氧气通风相比,流可能对初级生产和碳出口的贡献较小.
微小的尺度对于通过高档连接的低频自然变化很重要.
微小的过程可以缓冲气候变化对生物地化学循环的负面影响.

结论:

精细规模过程的交叉规模效应的准确核算对于气候预测至关重要.
需要跨学科的努力来将微小规模的动态整合到大规模的生物地质化学模型中.
需要进一步的研究,才能充分理解和建模海洋生物地球化学中的多尺度相互作用.

关键词:

碳的碳是一个碳.气候变化气候变化气候变化气候变化,气候的变化.脱氧化是脱氧化的过程.的流动是的流动.平均状态状态状态在中等层次的旋转中,出现中等层次的.初级生产中的初级生产.亚米索尺度的前沿地区.上层级的反反可以得到.

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